Enhanced mixing and reaction through flow focusing in heterogeneous porous media

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Non-Fickian mixing: Temporal evolution of the scalar dissipation rate in heterogeneous porous media (2010, background): “Non-Fickian mixing occurs due to transverse diffusion when new interfaces are created by shearing of the plume [48].”
Impact of sampling volume on the probability density function of steady state concentration (2008, methodology): “For example, flow focussing in high-conductivity areas enhances solute mixing [ Werth et al., 2006 ], which is a higherorder effect.”
Expanding the role of reactive transport models in critical zone processes (2017, background): “…have shown that solute transport into and out of these interfaces—often determined by transverse mixing or diffusive fluxes—plays a key role in reaction extent (Cirpka et al., 1999; Cirpka and Valocchi, 2007; Janot et al., 2016; Jose and Cirpka, 2004; Luo and Cirpka, 2008; Werth et al., 2006).”